• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/32

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

32 Cards in this Set

  • Front
  • Back

What is the ITCZ?

The Inter Tropical Convection Zone, where the North-east and South-east trade winds come together

Why is there a Net surplus of energy at the equator?

Higher intensity of sunlight due to the higher angle of the sun

Why is there a Net deficit of energy at the poles?

Ice creates a higher albedo effect and the sun is at a low angle creating a low intensity of sunlight

What is the Coriolis effect?

The Earth's spinning causes wind to be diverted right into the N.Hemisphere and left in the S.Hemisphere

What is an Arid climate?

An area not affected by the ITCZ as much and is mostly subtropical anticyclone, usually desert

What type of seasons does this climate have?

Long dry season and short wet season

An example of an Arid Climate?

Timbuktu, Mali (16 degrees North)

Timbuktu's annual rainfall?

206mm

What is a Tropical Wet + Dry climate?

An area that has distinct wet and dry seasons and is affected by ITCZ for half the year, usually Grassland Savanna

An example of this?

Kano, Nigeria (12 degrees North)

Kano's annual rainfall?

812mm

What is an Equatorial climate?

An area that is always affected by the ITCZ, with a constant wet season, usually tropical forest

An example of this?

Lagos, Nigeria (6 degrees North)

Lagos's annual rainfall?

1464mm

Stage 1 of Hadley Cell at the equator?

High angle of sun means high insulation, leading the heating of the surface, heating the air above it due to conduction

Stage 2?

As the air decreases in density it becomes unstable and rises as thermals leading to low pressure at the surface

Stage 3?

As the air rises the pressure decreases meaning temperature does too due to adiabatic cooling

Stage 4?

As the temperature falls condensation occurs producing cumulonimbus clouds

Stage 5?

As the water vapour condenses, it releases latent heat which causes further vertical uplift, leading to bigger clouds

Stage 6?

Once the rising air reaches the tropopause, it cant rise anymore as there is a temperature inversion

Stage 7?

The air is then forced to diverge N+S towards the tropics

What happens at the tropics?(Stage 1)

As the cold air high in the atmosphere moves away from the equator it sinks because it is denser than the air around it

Stage 2?

The sinking air experiences adiabatic warming as pressure increases

Stage 3?

As the air sinks it creates high pressure areas at the surface called Subtropical Anticyclones

Stage 4?

When the air reaches the surface it diverges creating the trade winds which travel back to equator, causing more air to rise at the equator

Characteristics of Kano in March?

ITCZ over equator


Start of wet season


Hottest time

Characteristics of Kano in June?

Wet season as ITCZ is overhead


Cooler due to cloud cover


Hot+Wet

Characteristics of Kano in September?

End of wet season


Warming up

Characteristics of Kano in December?

Kano's dry season


Subtropical anticyclone


Coldest time of year as tilted away from the sun

When is Kano warmest?

March and April as least cloud cover

When is Kano wettest?

August at 290mm

How is Dodoma (Tanzania) different to Kano?

Dodoma is south of the equator so will have the ITCZ overhead at different times than Kano and will therefore have dry seasons when Kano has wet.


Temperatures are also lower has Dodoma has a higher altitude so has less convectional rainfall and is therefore cooler and drier